お知らせ • Sep 09
Zeb Nickel Corp. Reports Positive Results from the Independent Interpretation of its High-Power SpectremPlus™? Airborne Electromagnetic Survey over the Zeb Nickel Project, Limpopo, South Africa ZEB Nickel Corp. reported positive results from the independent interpretation of its high-power SpectremPlus™? airborne electromagnetic ("AEM") survey over the Zeb Nickel Project, Limpopo, South Africa. The AEM dataset has been integrated with the project's gravity and magnetic models to refine the geological framework and rank conductive anomalies along the ultramafic intrusive trend. Coherent conductive responses identified: The interpretation delineates multiple discrete, laterally persistent conductors after screening for cultural and stratigraphic effects, with several features coincident with magnetic trends and intrusive margins which is consistent with the Company's chonolith/feeder-style nickel sulphide model. 3-D integration strengthens the geological case: Combining AEM, gravity and magnetics supports a focused corridor where sulphide accumulation is considered most plausible within or adjacent to the ultramafic package. De-risking pathway defined: The Company is advancing a follow-up programme that will include ground-based electromagnetic methods, downhole EM and complementary techniques to refine geometry, depth and conductance prior to selecting locations for initial drill-testing. The interpretation of the recently completed Spectrem survey by Geofocus (Pty) Ltd. outlines several clear, late-time conductive zones that cluster along the edges of the ultramafic body, interpreted to be a chonolith, and in close proximity to the magnetic and gravity shells. This spatial pattern is exactly what company's chonolith/feeder model anticipates: nickel-copper-PGE sulphides commonly accumulate in 'trap' sites along basal contacts and feeder embayments, often slightly offset from the densest and most magnetic core of the intrusion. By integrating the EM with magnetics and gravity in 3-D, the company's narrowed targeting to a well-defined corridor where intrusion-related sulphide mineralisation is geologically plausible, while filtering out many responses more likely to reflect stratigraphy or surface effects. These results do not confirm mineralisation, but the alignment of independent datasets materially strengthens the technical case and provides a strong foundation for focused follow-up geophysics to refine geometry and prioritise drill-ready targets. TLate-time AEM response with conductor picks. The orange "cloud" shows a conductive zone detected by the EM survey. The red and blue outlines are earlier models of denser and more magnetic rock. The anomaly sits beside the Uitloop intrusion and close to those outlines, which fits how massive sulphides often occur: they tend to pool along the base or edges of an intrusion or in feeder embayments, slightly offset from the hardest, most magnetic core. This geometry is consistent with that setting, although it does not confirm mineralisation. To increase precision ahead of any drill selection, the Company will conduct a ground-based geophysical survey over selected targets. The work may include a combination of moving-loop and/or fixed-loop EM and limited complementary methods where appropriate. Ground-based surveys provide orientation-controlled, higher signal-to-noise measurements that enable constrained plate modelling of conductive bodies. This improves confidence in position, dip and strike, and helps eliminate compact, highly conducting sulphide targets from look-alikes such as banded iron formation, graphitic horizons, conductive weathering fronts or cultural coupling. In practical terms, follow-up geophysics reduces false positives, sharpens drill vectors and lowers the probability of unnecessary metres, thereby improving capital efficiency and technical outcomes. The completion of the AEM survey combined with the ground based geophysical work is a key step for the Company in identifying the semi massive-massive sulphide discovery. The Company are working closely with the Mining Rights and hope to be in a position to update shareholders soon. Upon successful awarding of the Mining Rights, the Company intends on embarking on an extensive drill programme to further prove up the deposit. The Company is finalising the scope and sequencing of the follow-up programme to further prove up the follow-up programme. お知らせ • Jul 11
Zeb Nickel Corp. Reports Assay Results and Geological Interpretations from A Two-Hole Drilling Programme at the Zeb Nickel Project in Limpopo, South Africa Zeb Nickel Corp. reported assay results and geological interpretations from a two-hole drilling programme at the Zeb Nickel Project in Limpopo, South Africa. Drilled vertically, the holes validate the Zeb geological model, and confirms the presence of thicker, higher-grade nickel-copper-PGE ("Ni-Cu-PGE") horizons beneath the historic open-pit resource and demonstrates that mineralisation remains open both along strike and at depth. Key Value Highlights. Two drillholes plus two def collections completed intersected mineralised material in both Zone 1 and Zone 2. Zone 2 Ni-Cu-PGE mineralisation confirmed to be present in a previously untested area beneath Zone 1, confirming the geological model. Thicker, higher-grade intervals beneath the historical resource. oreholes Z031 and Z033 successfully intersected Ni and Ni-Cu-PGE Mineralisation in Zones 1 and 2 respectively, while Z031 and its def collections also intersected what is interpreted as Zone 3 mineralisation. The assay results confirm the presence of thick, higher-grade Ni-Cu-PGEeralised intervals of varying grade beneath the historical resource envelope and confirm the continuity of mineralisation in line with previous intersections along strike. Importantly, the data provides strong evidence that the Ni-Cu-PGE property continues below Zone 1 and may fully extend beneath Zone 1, meaning that the area holds increased potential to host a significant Ni-Cu-PGE resource. Of particular significance is the consistent intersection of semi-massive sulphide mineralisation associated with Zone 3 in the central part of the Uitloop body, where a potential chonolith structure may link the Uitloop I and II bodies. This is an exciting development, as such a chonolith could host a larger, more continuous sulphide accumulation due to its structural setting and potential to channel enriched magmatic pulses during emplacement and develop a Ni-Cu-PGE rich massive sulphide. 3PGE+Au equals platinum+ palladium+ rhodium+ gold by fire assay with ICP-AES Finish; Total Ni assay by complete digestion, representing the silicate and sulfide portion of Ni; Additional drilling is required to determine true thickness; "Depth From", "Depth To" and " Sample Thickness" reported are depths fromsurface down the drill hole. These results validate the geological model and confirm that Zeb Nickel has the scale and grade to become a significant critical-metal asset. With mineralisation open in multiple directions, and several exciting targets identified from the recent airborne magnetic and gravity survey, are as excited as ever about the growth runway ahead and look forward to updating the market on further exploration plans. お知らせ • Jun 05
Zeb Nickel Corp. Reports the Results of an Independent 3-D Inversion of High-Resolution Aeromagnetic and Falcon™? Airborne Gravity Data over the Zeb Nickel Project in Limpopo Province, South Africa Zeb Nickel Corp. reported the results of an independent 3-D inversion of high-resolution aeromagnetic and Falcon™? airborne gravity data over the Zeb Nickel Project ("Zeb") in Limpopo Province, South Africa. The work, completed by Geofocus (Pty) Ltd, refines and expands upon the conduit-style sulphide model, identifying four discrete, high-density targets interpreted to represent potential accumulations of massive nickel-copper-PGE sulphide mineralisation. High-Priority Targets 1 & 2: Large, coincident gravity-magnetic anomalies directly beneath parallel lobes of the Uitloop chonolith, interpreted as feeder conduits where massive sulphides could pond. Depth Extension Confirmed: Modelling indicates dense zones from ~100 m to >800 m below surface, significantly deeper than historic drilling, underscoring the untested potential at depth. Model Corroborates Conduit System: The new inversion reinforces the vertically stacked, feeder-pipe architecture which forms the basis of the massive sulphide exploration model, with clear similarities to the nickel-producing Uitkomst Complex. These highlights confirm that multiple dense, magnetically susceptible bodies lie wholly within the Company's licence and validate the ultramafic feeder-conduit geological model that underpins Zeb's massive sulphide (Zone 3) exploration thesis. Importantly, the new modelling expands the search footprint, both laterally and to depths well beyond historic drilling, and delivers a suite of clearly defined, drill-ready targets. Where red and green volumes overlap, the signature could represent sulphide lenses encased in magnetic cumulate. These intersections are prime drill targets because density and magnetic contrast both support a sulphide interpretation. Red bodies slightly offset from the green conduit may be sulphide accumulations that migrated into deeper embayments or structural traps in the footwall dolomite; they are equally compelling and will need angled drill holes to test. Scale and depth. Lateral continuity of the green conduit across several kilometres confirms a long lived plumbing system capable of repeated magma throughput, a key condition for concentrating large amounts of sulphide. 3-D Integration: Import VOXI shells into Leapfrog™? for constrained modelling with existing drill data. Electromagnetic Survey Option: The Company is evaluating both ground and airborne EM surveys to further delineate and rank the identified targets prior to drilling, and mitigate the risk of drilling false anomalies. Target Ranking & Drill Design: Prioritise Targets 1, 2 and 4 for first-pass deep diamond holes (planned depth 600-1 000 m). Community & ESG Engagement: Initiate stakeholder consultations in the Mokopane region ahead of field mobilisation. お知らせ • Apr 16
ZEB Nickel Corp., Annual General Meeting, Jun 25, 2025 ZEB Nickel Corp., Annual General Meeting, Jun 25, 2025. お知らせ • Apr 11
Zeb Nickel Corp. Advances Exploration with High-Resolution Airborne Geophysics and Expert Interpretation Zeb Nickel Corp. announced the completion of a high-resolution airborne geophysical survey over its project area, conducted by Xcalibur Airborne Geophysics (Pty) Ltd. The survey incorporated both gravity and magnetic data, designed to enhance the company's understanding of the underlying geological structures. The airborne data, flown at no cost to Zeb Nickel, has enabled the company to access a comprehensive dataset without diluting shareholder value. This newly acquired dataset has confirmed key aspects of the company's geological model - particularly the presence of a long-lived ultramafic magmatic plumbing system connecting the Uitloop I and II bodies. The survey has further highlighted several major NE-SW fault zones, interpreted to be part of a regional fault network, that likely acted as magma conduits and trap sites for sulfide mineralisation. The airborne data strengthens Zeb Nickel's exploration thesis that multiple zones of sulfide mineralisation - disseminated, semi-massive and potentially massive - are vertically stacked and associated with a feeder system analogous to those at Ivanhoe Mines' Platreef Project and African Rainbow Minerals' Nkomati Nickel Mine hosted in the Uitkomst Intrusion. To deepen the interpretation and support drill targeting within Zone 2 and Zone 3, Zeb Nickel will be submitting the dataset to a consulting geophysical company who are a leading provider of geophysical solutions across Southern, Central and West Africa. The Company believes that this work will directly support the delineation of higher-grade Ni-Cu-PGE mineralisation in Zone 2, as well as the identification of potential massive sulfide zones in Zone 3, where recent data suggests similarities to the sulfide mineralisation style of the Uitkomst deposit. お知らせ • Dec 07
ZEB Nickel Corp. Announces Chief Executive Officer Changes ZEB Nickel Corp. announced that Mr. James Nieuwenhuys, the current non-executive Chairman, will be assuming the role of Chief Executive Officer from the current interim CEO, Mr. Richard Montjoie, effective immediately. Mr. Montjoie will continue in his role as VP Exploration and director. Mr. Nieuwenhuys, a seasoned mining executive has previously held numerous senior positions, most recently as Chief Executive Officer of Eurasia Mining PLC Mr. Nieuwenhuys was the Chief Operating Officer at Polyus Gold, Russia's largest gold miner; and formerly the Chief Executive Officer at South African Lesego Platinum Mining Limited. Mr. Nieuwenhuys has an engineering background and has also held senior executive positions at a number of EPC organisations, including SNC Lavalin, Bateman Projects and Bateman Diamonds. Mr. Nieuwenhuys has extensive experience in greenfield and brownfield exploration projects and transitioning these into world-class mines, and in his new role as CEO, will be well positioned to strategically drive the Company forward and create value for its shareholders. お知らせ • Jul 01
ZEB Nickel Corp., Annual General Meeting, Aug 29, 2023 ZEB Nickel Corp., Annual General Meeting, Aug 29, 2023. お知らせ • Feb 08
ZEB Nickel Corp. Announces Completion of Full Evaluation of the Results from Both the Phase 1 and Phase 2 Drilling Campaigns ZEB Nickel Corp. announced that the Company has now completed a full evaluation of the results from both the Phase 1 and Phase 2 drilling campaigns and related these results to all available historical information, updated the exploration model and produced a three-dimensional geological model of the project area. The Company has identified higher grade zones within the Lower Zone lithologies that host the historical nickel resource estimate as described in the Company's NI43-101. Much of the historical drilling stopped short of these higher-grade zones, and further drilling into these zones could result in an increase in the grade of the resource estimate hosted in these Lower Zone lithologies. The development of a three-dimensional geological model has allowed the Company to better focus the next phase of exploration, which will include infill drilling on the gold targets with the aim of declaring a resource on the gold mineralization. The next phase of drilling on the Zebediela project aims to: Allow for the declaration of a current NI43-101 resource statement on the historical nickel resource hosted within Lower Zone lithologies; Define more resources in the "indicated resource" category for the nickel resource hosted in Lower Zone lithologies, and potentially move some material into the "measured resource" category; Increase the overall grade and tonnage on the historical nickel resource by targeting the serpentinite and poikilitic harzburgite units, where higher nickel grades have been intersected by previous drilling; Increase the grade and tonnage within Critical Zone (Target 2) lithologies, which consists of material proven to be a shallower up-dip extension of Ivanhoe's 800 m deep Platreef on the adjacent property; Determine the extent of the high-grade mineralized nickel zone at the base of, and in the footwall to, the Lower Zone lithologies, which is contact style mineralization and may host semi-massive to massive Ni-PGE sulfide mineralization; and Conduct infill diamond drilling to test the extent of the gold discovery, as reported in news releases on September 19th, 2022 and March 15, 2022; The case for increased nickel grade within the Historical Resource: The historical resource is associated with the ultramafic Lower Zone body, which hosts the historical estimate. The nickel mineralization starts near surface and was tested to a depth of ~350 m and has a strike length of 3 km. The body dips southwestward (30-70°) and is in excess of 350 m thick. There are approximately 34 drillholes which have intersected this body, however, the majority of the historical holes are stopped in the middle of the body and did not test the full nickel mineralization potential of this body. This body was previously thought to be relatively homogenous in both lithologies and nickel mineralization. A recent investigation conducted by the Company's geologists has indicated that this body is not as homogeneous as previously interpreted. The body can be divided into four broad stratigraphic units, namely the Dunite Unit, the Serpentinised Dunite Unit, the Serpentinite Unit and the Poikilitic Harzburgite Unit. These four units have different abundances of sulfide mineralization and associated nickel sulfide mineralization. The Serpentinite and Poikilitic Harzburgite Units close to the base of the body have an increased sulfide content of 5% - 10% that are blebby and disseminated in nature. This means that higher nickel grades are often associated with the lower two sulfide-rich stratigraphic units. Based on these broad lithological units found in the body, the true potential of the nickel mineralization has not yet been tested (Figure 1). The units that contain the highest nickel grades have only been intersected in a few of the historical boreholes (e.g., Z015 and U1). The majority of the historical drillholes were stopped in the middle of the Serpentinised Dunite Unit and did not test for higher-grade Ni mineralization associated with the lower two units. Z015 intersected these lower units with 21,50 m @ 0,49% Ni (including 5,50 m @ 0,72% Ni). The more recent boreholes that were drilled through the entire Lower Zone stratigraphy, were drilled close to the sub-crop position of the Lower Zone, and due to the nature of the geometry of the Lower Zone intrusion, these boreholes did not intersect a well-developed Serpentinite Unit and Poikilitic Harzburgite Units as seen in Z015 and U1. On this basis, the infill drilling program will target the higher-grade mineralized zones downdip of the sub-crop position of the Lower Zone, rather than the shallow sub-crop mineralized packages intersected in the historical drilling.